Abstract.
Vegetation
restoration
is
one
of
the
most
effective
measures
to
control
runoff
and
sediment
by
human
management.
Nevertheless,
few
studies
have
been
undertaken
objectively
analyze
effectiveness
effects
plant
on
regional
water
availability,
especially,
in
mixed-cultivated
grasslands
alpine
degraded
hillsides.
In
this
research,
we
carried
out
in
situ
monitoring
using
micro-plots
investigate
impact
three
strategies,
combining
two
grass
species
per
plot
(three
total),
a
20-degree
slope
activation
volume
surface
soil
loss
hillsides
for
years
(2019,
2020
2022).
A
bare-soil
was
used
as
control.
The
findings
indicated
that
can
effectively
conserve
decrease
along
increasing
planting
ages.
Grass
community
Deschampsia
cespitosaPoa
pratensis
L.cv.
Qinghai
reducing
erosion.
From
2019
2022,
values
reduction
ratio
decreased
Elymus
nutans
(DE),
(PE),
(PD)
from
-79.3
%
-115.4
%,
-130.4
-156.1
-48.5
-87.6
respectively.
On
contrary,
mean
erosion
cultivated
communities
increased
-184.8
18.0
(in
DE),
-231.5
24.3
PE),
-139.3
31.9
PD),
respectively,
2022;
corresponding
concentration
also
-120.9
55.8
-from
112.4
59.7
-94.3
62.1
PD).
This
implied
protection
should
be
considered
priority
during
initial
stage
grassland
key
factors
affecting
were
rainfall
amount,
duration
intensity
(60-min
intensity).
We
conclude
results
study
serve
scientific
guides
design
efficient
policy
decisions
planning
vegetation
severely
hillside
grasslands.
International Soil and Water Conservation Research,
Год журнала:
2023,
Номер
12(3), С. 565 - 577
Опубликована: Ноя. 25, 2023
Global
climate
change
and
overgrazing
are
driving
shifts
in
the
plant
composition
of
grassland
communities,
which
may
profoundly
affect
function
ecosystems
regulating
runoff
soil
erosion.
Here,
we
examined
shift
effects
normal
hillslope
alpine
meadow
to
shrub
severely
degraded
states
on
sediment
generation
under
natural
rainfall
conditions,
determined
contributions
properties
changes
erodibility,
by
situ
experiment
monitoring
Qinghai-Tibetan
Plateau.
The
results
showed
that
into
state,
mean
weight
diameter,
saturated
hydraulic
conductivity,
cohesion
erodibility
K-factor
at
topsoil
decreased
70.3%,
73.1%,
80.3%
−13.1%,
respectively,
when
meadows
they
reduced
49.1%,
−1.3%,
49.4%,
−8.3%,
respectively.
Runoff
loss
significantly
changed
-
40.0%
177.8%
shifted
a
while
+
65.0%
+77.8%
state.
Our
findings
highlight
two
divergent
both
increased
compared
meadows.
Overall,
our
indicate
exacerbated
These
obtained
here
offer
novel
perspective
regulation
erosion
ecosystem.
Water,
Год журнала:
2024,
Номер
16(4), С. 571 - 571
Опубликована: Фев. 15, 2024
Retrogressive
thaw
slumps
(RTSs)
are
becoming
more
common
on
the
Qinghai-Tibet
Plateau
as
permafrost
thaws,
but
hydraulic
properties
of
have
not
been
extensively
studied.
To
fill
this
knowledge
gap,
we
used
“space-for-time
substitution
method”
to
differentiate
three
stages
RTSs:
original
grassland,
collapsing,
and
collapsed.
Our
study
included
on-site
investigations,
measurements
in
laboratory,
measured
simulated
analyses
soil
water
retention
curves
estimated
hydrological
properties.
findings
show
that
were
highly
consistent
across
RTSs,
indicating
accuracy
Van
Genuchten
model
reproducing
parameters
for
different
RTSs.
The
grassland
stage
had
highest
content
due
its
high
organic
carbon
(SOC)
fine-textured
micropores.
In
contrast,
collapsed
higher
compared
collapsing
stage,
primarily
increased
proportions
micropores,
SOC
content,
lower
bulk
density
(BD).
From
there
significant
changes
structure
each
RTS
site,
which
resulted
a
decrease
an
increase
BD
general.
However,
absence
compaction
led
subsequent
accumulation
matter,
increasing
content.
Changes
field
capacity,
permanent
wilting
point,
micropore
distribution
aligned
with
variations
These
highlight
importance
managing
mitigate
adverse
effects
freeze-thaw
cycles
stability
at
collapse
Effective
management
strategies
may
include
incorporating
reducing
compaction,
maintaining
optimal
Further
research
is
needed
determine
most
suitable
practices
types
environmental
conditions.
Geoderma,
Год журнала:
2024,
Номер
443, С. 116828 - 116828
Опубликована: Фев. 21, 2024
Artificial
grassland
is
considered
an
effective
measure
for
restoring
severely
degraded
in
alpine
areas
and
has
been
widely
applied
on
the
Qinghai-Tibetan
Plateau.
However,
specific
effects
of
artificial
restoration
degradation
slope
runoff
sediment
yield
are
still
poorly
understood.
In
this
study,
we
investigated
process
three
areas:
meadow
(AM),
a
(BL),
that
was
restored
by
(AG).
Our
findings
revealed
AG
significantly
lower
than
both
AM
BL,
with
reductions
95.59%
88.40%,
respectively.
The
reduced,
21.77%
90.54%
compared
to
Nevertheless,
concentration
27.22
3.26
times
higher
study
provides
clear
evidence
plant
soil
properties
play
crucial
role
driving
erosion
processes
BL.
Specifically,
inhibiting
yield.
This
inhibition
attributed
modification
conditions
interception
rainfall,
which
were
facilitated
recovery
vegetation
coverage
increased
input
organic
matter.
These
have
significant
implications
meadows
prevention
efforts
Hydrology and earth system sciences,
Год журнала:
2024,
Номер
28(16), С. 3947 - 3961
Опубликована: Авг. 28, 2024
Abstract.
Vegetation
restoration
is
among
the
most
effective
measures
for
controlling
runoff
and
soil
erosion
resulting
from
human
activities.
Nevertheless,
few
studies
have
been
undertaken
to
analyze
effects
of
grassland
on
maintaining
local
runoff,
especially
alpine
degraded
hillsides
where
mixed-cultivation
grasslands
predominate.
In
this
research,
plots
were
established
investigate
impact
three
grasslands,
each
sowing
two
grass
species
per
plot
a
20°
slope:
Deschampsia
cespitosa
Elymus
nutans
(DE),
Poa
pratensis
L.
cv.
Qinghai
(PE),
(PD).
The
activation
volume
surface
magnitude
loss
over
3
years
(2019,
2020,
2022)
assessed.
A
severely
meadow
(SDM)
was
used
as
control.
findings
indicated
that
can
effectively
maintain
reduce
planting
age
increases.
Between
2019
2022,
values
average
depth
DE,
PE,
PD,
SDM
0.47,
0.55,
0.45,
0.27
mm,
respectively.
Despite
increase
in
favored
conservation:
net
losses
unit
area
1.4,
1.3,
1.9
times
greater
than
those
key
factors
affecting
rainfall
amount,
duration,
intensity
(60
min
intensity).
We
conclude
results
study
serve
scientific
guides
formulate
efficient
policy
decisions
planning
vegetation
hillside
meadows.
To
improve
effectiveness
restoration,
we
suggest
protective
should
be
prioritized
during
initial
stage
cultivated
grasslands.
Abstract.
Vegetation
restoration
is
one
of
the
most
effective
measures
to
control
runoff
and
sediment
by
human
management.
Nevertheless,
few
studies
have
been
undertaken
objectively
analyze
effectiveness
effects
plant
on
regional
water
availability,
especially,
in
mixed-cultivated
grasslands
alpine
degraded
hillsides.
In
this
research,
we
carried
out
situ
monitoring
using
micro-plots
investigate
impact
three
strategies,
combining
two
grass
species
per
plot
(three
total),
a
20-degree
slope
activation
volume
surface
soil
loss
hillsides
for
years
(2019,
2020
2022).
A
bare-soil
was
used
as
control.
The
findings
indicated
that
can
effectively
conserve
decrease
along
increasing
planting
ages.
Grass
community
Deschampsia
cespitosa
Poa
pratensis
L.cv.
Qinghai
reducing
erosion.
From
2019
2022,
values
reduction
ratio
decreased
Elymus
nutans
(DE),
(PE),
(PD)
from
-79.3
%
-115.4
%,
-130.4
-156.1
-48.5
-87.6
respectively.
On
contrary,
mean
erosion
cultivated
communities
increased
-184.8
18.0
(in
DE),
-231.5
24.3
PE),
-139.3
31.9
PD),
respectively,
2022;
corresponding
concentration
also
-120.9
55.8
-from
112.4
59.7
-94.3
62.1
PD).
This
implied
protection
should
be
considered
priority
during
initial
stage
grassland
key
factors
affecting
were
rainfall
amount,
duration
intensity
(60-min
intensity).
We
conclude
results
study
serve
scientific
guides
design
efficient
policy
decisions
planning
vegetation
severely
hillside
grasslands.
Retrogressive
thaw
slumps
(RTSs)
are
becoming
more
common
on
the
Qinghai-Tibet
Plateau
as
permafrost
thaws,
but
hydraulic
characteristics
of
these
have
not
been
extensively
studied.
To
fill
this
knowledge
gap,
we
used
''space-for-time
substitution
method''
to
differentiate
three
stages
RTSs:
original
grassland,
collapsing,
and
collapsed.
Our
study
included
on-site
investigations,
measurements,
simulated
analyses
soil
water
characteristics,
environmental
factors,
hydrological
properties.
findings
show
that
measurements
were
highly
consistent
across
RTSs,
indicating
accuracy
V-G
model
in
reproducing
parameters
for
different
RTSs.
The
grassland
stage
had
highest
retention
content
due
its
high
SOM
fine-textured
micropores.
In
contrast,
collapsed
higher
compared
collapsing
stage,
primarily
increased
proportions
micropores,
content,
lower
bulk
density
(BD).
Freeze-thaw
cycles
a
significant
impact
texture
structure
resulting
decrease
an
increase
BD.
However,
absence
compaction
led
subsequent
accumulation
organic
matter,
increasing
content.
Changes
field
capacity
(FC),
permanent
wilting
point
(PWP),
micropore
distribution
aligned
with
variations
content.These
highlight
importance
managing
mitigate
adverse
effects
freeze-thaw
stability
at
Effective
management
strategies
may
include
incorporating
reducing
compaction,
maintaining
optimal
Further
research
is
needed
determine
most
suitable
practices
types
conditions.